THE LOWER CAMBRIAN BOUNDARY IN INNER AREAS OF THE NORTH SIBERIAN PLATFORM

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dc.contributor.author Khomentovskii V.V.
dc.contributor.author Karlova G.A.
dc.contributor.author Fedorov A.B.
dc.date.accessioned 2020-12-31T03:44:30Z
dc.date.available 2020-12-31T03:44:30Z
dc.date.issued 1998
dc.identifier https://elibrary.ru/item.asp?id=13298228
dc.identifier.citation Stratigraphy and Geological Correlation, 1998, , 1, 1-9
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/21849
dc.description.abstract The Vendian-Cambrian sequences recovered by boreholes K-203 and K-204 and by the deep Eiik Hole 343-0 in the North Siberian platform yielded abundant small-shelled fossils characteristic of the N. sunnaginicus Zone of the Tommotian Stage and also of P. antiqua and A. trisulcatus zones of the Nemakit-Daldynian Stage. These sequences appear to be more fossiliferous than the coeval sequence of the reference Markha borehole, which is used for the correlation of natural exposures in the northern part of Siberia with the borehole sections in its inner part. New data enable us to use the recognized stratigraphic subdivisions in the inner oil-and-gas provinces of the Siberian platform and to outline the elaboration method of the general stratigraphic scale for the Vendian-Cambrian boundary beds.
dc.subject Cambrian en
dc.title THE LOWER CAMBRIAN BOUNDARY IN INNER AREAS OF THE NORTH SIBERIAN PLATFORM
dc.type Статья
dc.subject.age Paleozoic::Cambrian en
dc.subject.age Палеозой::Кембрийская ru


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